Krivitskiy P Ye, Larionova N V, Baklanova Yu V, Aidarkhanov А O, Lukashenko S N
Institute of Radiation Safety and Ecology, NNC, Kurchatov, Kazakhstan.
Institute of Radiation Safety and Ecology, NNC, Kurchatov, Kazakhstan.
J Environ Radioact. 2022 Aug;249:106893. doi: 10.1016/j.jenvrad.2022.106893. Epub 2022 May 12.
The paper provides study of the radioactive contamination of near-surface soil at the Sary-Uzen site in the Semipalatinsk test site (STS). Increased values of natural radionuclides in the studied area were not detected, which indicates the absence of possible geochemical anomalies that could create an elevated radiation background. Radioactive contamination by technogenic radionuclides is caused by two factors. The first factor is fallout of radioisotopes from the atmosphere because of an explosion on September 24, 1951 at the "Experimental field" site. The fallout plume extended from the north-western part of the site to the very south. The range of activity concentration values for Am in soil varies from <0.3 Bq/kg to 390 Bq/kg, with an average value of 5 Bq/kg; for Cs from <1.1 Bq/kg to 330 Bq/kg, with an average value of 55 Bq/kg. A second, but more significant factor is the fallout of radioisotopes due to underground nuclear tests with radioactive release that took place in boreholes on the site itself. The largest area of contamination (about 8 km) is the fallout from testing borehole No. 101 (Am to 920 Bq/kg and Cs to 12150 Bq/kg).
该论文对塞米巴拉金斯克试验场(STS)萨雷 - 乌曾场址近地表土壤的放射性污染进行了研究。在所研究区域未检测到天然放射性核素值升高的情况,这表明不存在可能造成辐射本底升高的地球化学异常。人为放射性核素造成的放射性污染由两个因素导致。第一个因素是1951年9月24日在“试验场”场址发生爆炸后,大气中放射性同位素的沉降。沉降羽状物从场址的西北部延伸至最南端。土壤中镅的活度浓度值范围为<0.3贝克勒尔/千克至390贝克勒尔/千克,平均值为5贝克勒尔/千克;铯的活度浓度值范围为<1.1贝克勒尔/千克至330贝克勒尔/千克,平均值为55贝克勒尔/千克。第二个但更重要的因素是由于该场址自身钻孔中进行的伴有放射性释放的地下核试验导致的放射性同位素沉降。污染面积最大的区域(约8千米)是101号试验钻孔的沉降区域(镅达920贝克勒尔/千克,铯达12150贝克勒尔/千克)。